12.07.2015 Views

The Soils of Elgin County - Agriculture and Agri-Food Canada

The Soils of Elgin County - Agriculture and Agri-Food Canada

The Soils of Elgin County - Agriculture and Agri-Food Canada

SHOW MORE
SHOW LESS
  • No tags were found...

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

tillage practices, particularly no-till practices forfall crops, should be considered for these soils.Wattford <strong>Soils</strong> (WF)L<strong>and</strong>form <strong>and</strong> TopographyWattford soils have developed on blankets <strong>of</strong>medium to coarse textured lacustrine materialswhich frequently have been modified by. wind .<strong>The</strong>y usually occur on upper <strong>and</strong> crest slopepositions in l<strong>and</strong>scapes which have nearly level orvery gently undulating topography. Occasionallythey occur in l<strong>and</strong>scapes which have very gentlyundulating or hummocky topography. Slopesrange from 2 to 15%, with slopes <strong>of</strong> 2 to 5 % beingmost common.Soil Moisture CharacteristicsWattford soils are well drained <strong>and</strong>moderately permeable. <strong>The</strong>yhave moderate waterholding capacities, <strong>and</strong> droughtiness is usually alimitation . Surface run<strong>of</strong>f is generally moderate toslow, but can be rapid on steeper slopes where thesoil materials tend to have high very fine s<strong>and</strong> orsilt contents .General Soil Characteristics<strong>The</strong> Ap <strong>and</strong> Bm horizons usually have -veryfine s<strong>and</strong>y loam, fine s<strong>and</strong>y loam, or loamy fines<strong>and</strong> textures. Clay enriched Bt horizons, whichfrequently have fine s<strong>and</strong>y loam or very fines<strong>and</strong>y loam texures, commonly occur above thecalcareous Ck horizons . <strong>The</strong> Ck horizons aremore variable in texture than the upper horizons .Common textures <strong>of</strong> those horizons are very fines<strong>and</strong>y loam, fine s<strong>and</strong>y loam, loamy fine s<strong>and</strong>,loamy very fine s<strong>and</strong>, very fine s<strong>and</strong>, <strong>and</strong> fines<strong>and</strong>.Soil reaction ranges from medium acid toneutral in the Ap horizons, to mildly alkaline inthe Ck horizons . Soil classification is typicallyBrunisolic Gray Brown Luvisol .Soil VariabilityWattford soil materials may be uniformthroughout the pr<strong>of</strong>ile, or they may be variable<strong>and</strong> consist <strong>of</strong> layers <strong>of</strong> medium <strong>and</strong> coarsetextured materials. Many Wattford soils haveuniform fine s<strong>and</strong> textures, with 30% or more <strong>of</strong>the s<strong>and</strong> content being very fine in size .Wattford soils <strong>of</strong>ten occur in combination withNorm<strong>and</strong>ale (NO) soils .L<strong>and</strong> Use/Management CommentsWattford soils are rated Class 2M for commonfield crops when topography is not not alimitation . If the surface slopes are not too steep,they are suitable for a wide range <strong>of</strong> special crops .<strong>The</strong>ir suitability for many special crops increasesif supplemental irrigation is carried out.Suitability ratings for selected special crops aregiven in Tables 6, 7, <strong>and</strong> 8 .Wattford soils are susceptible to both wind<strong>and</strong> water erosion . Acrop rotation which includesa forage crop, planting cover crops, establishingwindbreaks, <strong>and</strong> maintaining high crop residuelevels will aid in reducing the risk <strong>of</strong> erosion .Conservation tillage practices should beconsidered for these soils.Wauseon <strong>Soils</strong> (WU)L<strong>and</strong>form <strong>and</strong> TopographyWauseon soils have developed on 40 to 100cmthick veneers <strong>of</strong> coarse textured lacustrinematerials which are underlain by fine to very finetextured lacustrine materials . <strong>The</strong>y usually occuron lower slope positions <strong>and</strong> in depressions inl<strong>and</strong>scapes which have nearly level or very gentlyundulating topography. Slopes are less than 2% .Soil Moisture CharacteristicsWauseon soils are poorly drained . <strong>The</strong> uppercoarse textured materials are rapidly permeable,but permeability is slow in the lower fine to veryfine textured materials. <strong>The</strong> poor drainageconditions associated with these soils if <strong>of</strong>tencaused by high water table levels which occurwithin 50 cm <strong>of</strong> the surface for prolonged periodseach year. Wauseon soils have low water holdingcapacities in the upper materials, <strong>and</strong> high waterholding capacities in the lower materials . Surfacerun<strong>of</strong>f is slow.General Soil Characteristics<strong>The</strong> Ap <strong>and</strong> Bg horizons occur in the uppercoarse textured materials <strong>and</strong> usually have fines<strong>and</strong>y loam, s<strong>and</strong>y loam, or loamy fine s<strong>and</strong>textures . Occasionally calcareous Ckg horizons,which frequently have fine s<strong>and</strong> or loamy fines<strong>and</strong> textures, also occur in the upper materials.<strong>The</strong> lower finer textured materials usually consist<strong>of</strong> calcareous IICkg horizons which have silty clayor silty clay loam textures .Gray gley colours are dominant within thepr<strong>of</strong>ile, <strong>and</strong> prominent dark yellowish brown tolight olive brown mottles are also present. Soil52

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!